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Search Results (1,413)

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23 pages, 949 KiB  
Article
Performance Improvement of a Standalone Hybrid Renewable Energy System Using a Bi-Level Predictive Optimization Technique
by Ayman Al-Quraan, Bashar Al-Mharat, Ahmed Koran and Ashraf Ghassab Radaideh
Sustainability 2025, 17(2), 725; https://doi.org/10.3390/su17020725 (registering DOI) - 17 Jan 2025
Viewed by 230
Abstract
A standalone hybrid renewable energy system (HRES) that combines different types of renewable energy sources and storages offers a sustainable energy solution by reducing reliance on fossil fuels and minimizing greenhouse gas emissions. In this paper, a standalone hybrid renewable energy system (HRES) [...] Read more.
A standalone hybrid renewable energy system (HRES) that combines different types of renewable energy sources and storages offers a sustainable energy solution by reducing reliance on fossil fuels and minimizing greenhouse gas emissions. In this paper, a standalone hybrid renewable energy system (HRES) involving wind turbines, photovoltaic (PV) modules, diesel generators (DG), and battery banks is proposed. For this purpose, it is necessary to size and run the proposed system for feeding a residential load satisfactorily. For two typical winter and summer weeks, weather historical data, including irradiance, temperature, wind speed, and load profiles, are used as input data. The overall optimization framework is formulated as a bi-level mixed-integer nonlinear programming (BMINLP) problem. The upper-level part represents the sizing sub-problem that is solved based on economic and environmental multi-objectives. The lower-level part represents the energy management strategy (EMS) sub-problem. The EMS task utilizes the model predictive control (MPC) approach to achieve optimal technoeconomic operational performance. By the definition of BMINLP, the EMS sub-problem is defined within the constraints of the sizing sub-problem. The MATLAB R2023a environment is employed to execute and extract the results of the entire problem. The global optimization solver “ga” is utilized to implement the upper sub-problem while the “intlinprg” solver solves the lower sub-problem. The evaluation metrics used in this study are the operating, maintenance, and investment costs, storage unit degradation, and the number of CO2 emissions. Full article
26 pages, 11476 KiB  
Article
Evaluating the Accuracy of the ERA5 Model in Predicting Wind Speeds Across Coastal and Offshore Regions
by Mohamad Alkhalidi, Abdullah Al-Dabbous, Shoug Al-Dabbous and Dalal Alzaid
J. Mar. Sci. Eng. 2025, 13(1), 149; https://doi.org/10.3390/jmse13010149 - 16 Jan 2025
Viewed by 294
Abstract
Accurate wind speed and direction data are vital for coastal engineering, renewable energy, and climate resilience, particularly in regions with sparse observational datasets. This study evaluates the ERA5 reanalysis model’s performance in predicting wind speeds and directions at ten coastal and offshore stations [...] Read more.
Accurate wind speed and direction data are vital for coastal engineering, renewable energy, and climate resilience, particularly in regions with sparse observational datasets. This study evaluates the ERA5 reanalysis model’s performance in predicting wind speeds and directions at ten coastal and offshore stations in Kuwait from 2010 to 2017. This analysis reveals that ERA5 effectively captures general wind speed patterns, with offshore stations demonstrating stronger correlations (up to 0.85) and higher Perkins Skill Score (PSS) values (up to 0.94). However, the model consistently underestimates wind variability and extreme wind events, especially at coastal stations, where correlation coefficients dropped to 0.35. Wind direction analysis highlighted ERA5’s ability to replicate dominant northwest wind patterns. However, it reveals notable biases and underrepresented variability during transitional seasons. Taylor diagrams and error metrics further emphasize ERA5’s challenges in capturing localized dynamics influenced by land-sea interactions. Enhancements such as localized calibration using high-resolution datasets, hybrid models incorporating machine learning techniques, and long-term monitoring networks are recommended to improve accuracy. By addressing these limitations, ERA5 can more effectively support engineering applications, including coastal infrastructure design and renewable energy development, while advancing Kuwait’s sustainable development goals. This study provides valuable insights into refining reanalysis model performance in complex coastal environments. Full article
(This article belongs to the Section Coastal Engineering)
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<p>Locations of 10 meteorological stations in the state of Kuwait.</p>
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<p>Measured seasonal wind rose diagrams for 10 stations (St01–St10) showing wind directional distribution and speed magnitude across different seasons.</p>
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<p>Measured seasonal wind rose diagrams for 10 stations (St01–St10) showing wind directional distribution and speed magnitude across different seasons.</p>
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<p>The scatter plot compares the measured wind speeds versus ERA5 predicted wind speeds across all ten stations. Data points are color-coded by station to illustrate the model’s performance variability in different geographical locations. The dashed line represents the perfect agreement between measured and predicted values.</p>
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<p>Box plots showing wind speed distribution for coastal and offshore stations. The circles represent outliers (extreme events) located beyond 1.5<span class="html-italic">IQR</span> of the whisker.</p>
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<p>Box plots showing the monthly variability of wind speeds for coastal and offshore stations. The circles represent outliers (extreme events) located beyond 1.5<span class="html-italic">IQR</span> of the whisker.</p>
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<p>Seasonal (<b>top</b>) and monthly (<b>bottom</b>) average Pearson correlation coefficients between measured and ERA5 wind speed data for the ten stations.</p>
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<p>Taylor diagram showing the comparison between ERA5 and observed wind speed data for coastal stations. The Pearson correlation coefficient is on the polar axis, the red dashed circles represent the normalized RMSE, and the horizontal and vertical axes represent the <span class="html-italic">σ</span><sub>n</sub>.</p>
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<p>Taylor diagram showing the comparison between ERA5 and observed wind speed data for offshore stations. The Pearson correlation coefficient is on the polar axis, the red dashed circles represent the normalized RMSE, and the horizontal and vertical axes represent the <span class="html-italic">σ</span><sub>n</sub>.</p>
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<p>Comparison of measured and modeled wind speed frequency distributions across the stations with Perkins Skill Score (PSS). The shaded blue areas represent the overlap between measured (dashed blue lines) and modeled (solid red lines) distribution.</p>
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<p>BSS evaluation across stations (St01–St10), showing the model’s performance relative to the baseline (BSS = 0). Positive BSS values indicate that the model outperforms the reference approach, while negative values highlight underperformance.</p>
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<p>ERA5 seasonal wind rose diagrams for the ten stations (st01–st10) showing wind directional distribution and speed magnitude across different seasons.</p>
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<p>ERA5 seasonal wind rose diagrams for the ten stations (st01–st10) showing wind directional distribution and speed magnitude across different seasons.</p>
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21 pages, 10261 KiB  
Article
Super Typhoons Simulation: A Comparison of WRF and Empirical Parameterized Models for High Wind Speeds
by Haihua Fu, Yan Wang, Yanshuang Xie, Chenghan Luo, Shaoping Shang, Zhigang He and Guomei Wei
Appl. Sci. 2025, 15(2), 776; https://doi.org/10.3390/app15020776 - 14 Jan 2025
Viewed by 372
Abstract
As extreme forms of tropical cyclones (TCs), typhoons pose significant threats to both human society and the natural environment. To better understand and predict their behavior, scientists have relied on numerical simulations. Current typhoon modeling primarily falls into two categories: (1) complex simulations [...] Read more.
As extreme forms of tropical cyclones (TCs), typhoons pose significant threats to both human society and the natural environment. To better understand and predict their behavior, scientists have relied on numerical simulations. Current typhoon modeling primarily falls into two categories: (1) complex simulations based on fluid dynamics and thermodynamics, and (2) empirical parameterized models. Most comparative studies on these models have focused on wind speed below 50 m/s, with fewer studies addressing high wind speed (above 50 m/s). In this study, we design and compare four different simulation approaches to model two super typhoons: Typhoon Surigae (2102) and Typhoon Nepartak (1601). These approaches include: (1) The Weather Research and Forecasting (WRF) model simulation driven by NCEP Final Operational Global Analysis data (FNL), (2) WRF simulation driven by the fifth generation of the European Centre for Medium-Range Weather Forecasts (ECMWF) reanalysis data (ERA5), (3) the empirical parameterized Holland model, and (4) the empirical parameterized Jelesnianski model. The simulated wind fields were compared with the measured wind data from The Soil Moisture Active Passive (SMAP) platform, and the resulting wind fields were then used as inputs for the Simulating WAves Nearshore (SWAN) model to simulate typhoon-induced waves. Our findings are as follows: (1) for high wind speeds, the performance of the empirical models surpasses that of the WRF simulations; (2) using more accurate driving wind data improves the WRF model’s performance in simulating typhoon wind speeds, and WRF simulations excel in representing wind fields in the outer regions of the typhoon; (3) careful adjustment of the maximum wind speed radius parameter is essential for improving the accuracy of the empirical models. Full article
(This article belongs to the Section Marine Science and Engineering)
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<p>Workflow Diagram for WRF Model Simulation.</p>
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<p>Typhoon tracks and intensity information recorded by the CMA dataset.</p>
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<p>Simulation domain in the WRF model. The red lines show the d01 area, the blue lines show the d02 area, the solid line represents the simulation domain for Typhoon Surigae, and the dashed line represents the simulation domain for Typhoon Nepartak.</p>
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<p>SWAN simulation domains. The red line shows the SWAN area of typhoon Surigae, and the blue line shows the SWAN area of typhoon Nepartak.</p>
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<p>Wind field for Typhoon Surigae at 09:00 on 17 April 2021. (<b>a</b>) shows the simulation driven by FNL data using WRF, (<b>b</b>) shows the simulation driven by ERA5 data using WRF, (<b>c</b>) shows the simulation using the Holland empirical parameter typhoon model, (<b>d</b>) shows the simulation using the Jelesnianski empirical parameter typhoon model, and (<b>e</b>) shows the SMAP data.</p>
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<p>Wind field for Typhoon Surigae at 21:00 on 17 April 2021. (<b>a</b>) shows the simulation driven by FNL data using WRF, (<b>b</b>) shows the simulation driven by ERA5 data using WRF, (<b>c</b>) shows the simulation using the Holland empirical parameter typhoon model, (<b>d</b>) shows the simulation using the Jelesnianski empirical parameter typhoon model, and (<b>e</b>) shows the SMAP data.</p>
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<p>Wind field simulation results for Typhoon Nepartak at 09:00 on 4 July 2016. (<b>a</b>) shows the simulation driven by FNL data using WRF, (<b>b</b>) shows the simulation driven by ERA5 data using WRF, (<b>c</b>) shows the simulation using the Holland empirical parameter typhoon model, (<b>d</b>) shows the simulation using the Jelesnianski empirical parameter typhoon model, and (<b>e</b>) shows the SMAP data.</p>
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<p>Wind field simulation results for Typhoon Nepartak at 22:00 on 6 July 2016. (<b>a</b>) shows the simulation driven by FNL data using WRF, (<b>b</b>) shows the simulation driven by ERA5 data using WRF, (<b>c</b>) shows the simulation using the Holland empirical parameter typhoon model, (<b>d</b>) shows the simulation using the Jelesnianski empirical parameter typhoon model, and (<b>e</b>) shows the SMAP data.</p>
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<p>Comparison of Typhoon Surigae Center Path. (<b>a</b>) shows the Typhoon Surigae. (<b>b</b>) shows the Typhoon Nepartak. The red line represents CMA recorded data, the green line indicates the WRF simulation driven by ERA5, and the blue line represents the WRF simulation driven by FNL.</p>
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<p>Comparison of Typhoon Surigae Intensity Simulations. (<b>a</b>) shows the comparison of extreme wind speeds, (<b>b</b>) shows the minimum surface pressure. The black line represents the WRF simulation driven by FNL, the blue line represents the WRF simulation driven by ERA5, the green line corresponds to the empirical parameterized typhoon model Holland, the yellow line corresponds to the empirical parameterized typhoon model Jelesnianski, the purple dots represent the maximum wind speed data recorded by CMA, and the red triangles represent the maximum wind speed data from SMAP.</p>
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<p>Comparison of Typhoon Nepartak Intensity Simulations. (<b>a</b>) shows the comparison of extreme wind speeds, (<b>b</b>) shows the minimum surface pressure. The black line represents the WRF simulation driven by FNL, the blue line represents the WRF simulation driven by ERA5, the green line corresponds to the empirical parameterized typhoon model Holland, the yellow line corresponds to the empirical parameterized typhoon model Jelesnianski, the purple dots represent the maximum wind speed data recorded by CMA, and the red triangles represent the maximum wind speed data from SMAP.</p>
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<p>Comparison of Significant Wave Height Simulations in Typhoon Surigae. (<b>a</b>) shows the WRF simulation driven by FNL, (<b>b</b>) shows the WRF simulation driven by ERA5, (<b>c</b>) shows the empirical parameterized typhoon model Holland, and (<b>d</b>) shows the empirical parameterized typhoon model Jelesnianski.</p>
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<p>The location of the reference point near the coast, and the time series of significant wave height at this point for Typhoon Surigae, the red point is the location of the reference point, the red line represents the FNL-driven WRF simulation, the blue line represents the ERA5-driven WRF simulation, the green line corresponds to the Holland case, and the yellow line corresponds to the Jelesnianski case.</p>
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<p>Comparison of Significant Wave Height Simulations in Typhoon Nepartak. (<b>a</b>) shows the WRF simulation driven by FNL, (<b>b</b>) shows the WRF simulation driven by ERA5, (<b>c</b>) shows the empirical parameterized typhoon model Holland, and (<b>d</b>) shows the empirical parameterized typhoon model Jelesnianski.</p>
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<p>The location of the reference point near the coast, and the time series of significant wave height at this point for Typhoon Nepartak, the red point is the location of the reference point, the red line represents the FNL-driven WRF simulation, the blue line represents the ERA5-driven WRF simulation, the green line corresponds to the Holland case, and the yellow line corresponds to the Jelesnianski case.</p>
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32 pages, 11641 KiB  
Article
The Performance of a High-Resolution WRF Modelling System in the Simulation of Severe Tropical Cyclones over the Bay of Bengal Using the IMDAA Regional Reanalysis Dataset
by Thatiparthi Koteshwaramma, Kuvar Satya Singh and Sridhara Nayak
Climate 2025, 13(1), 17; https://doi.org/10.3390/cli13010017 - 13 Jan 2025
Viewed by 330
Abstract
Extremely severe cyclonic storms over the North Indian Ocean increased by approximately 10% during the past 30 years. The climatological characteristics of tropical cyclones for 38 years were assessed over the Bay of Bengal (BoB). A total of 24 ESCSs formed over the [...] Read more.
Extremely severe cyclonic storms over the North Indian Ocean increased by approximately 10% during the past 30 years. The climatological characteristics of tropical cyclones for 38 years were assessed over the Bay of Bengal (BoB). A total of 24 ESCSs formed over the BoB, having their genesis in the southeast BoB, and the intensity and duration of these storms have increased in recent times. The Advanced Research version of the Weather Research and Forecasting (ARW) model is utilized to simulate the five extremely severe cyclonic storms (ESCSs) over the BoB during the past two decades using the Indian Monsoon Data Assimilation and Analysis (IMDAA) data. The initial and lateral boundary conditions are derived from the IMDAA datasets with a horizontal resolution of 0.12° × 0.12°. Five ESCSs from the past two decades were considered: Sidr 2007, Phailin 2013, Hudhud 2014, Fani 2019, and Amphan 2020. The model was integrated up to 96 h using double-nested domains of 12 km and 4 km. Model performance was evaluated using the 4 km results, compared with the available observational datasets, including the best-fit data from the India Meteorological Department (IMD), the Tropical Rainfall Measuring Mission (TRMM) satellite, and the Doppler Weather Radar (DWR). The results indicated that IMDAA provided accurate forecasts for Fani, Hudhud, and Phailin regarding the track, intensity, and mean sea level pressure, aligning well with the IMD observational datasets. Statistical evaluation was performed to estimate the model skills using Mean Absolute Error (MAE), the Root Mean Square Error (RMSE), the Probability of Detection (POD), the Brier Score, and the Critical Successive Index (CSI). The calculated mean absolute maximum sustained wind speed errors ranged from 8.4 m/s to 10.6 m/s from day 1 to day 4, while mean track errors ranged from 100 km to 496 km for a day. The results highlighted the prediction of rainfall, maximum reflectivity, and the associated structure of the storms. The predicted 24 h accumulated rainfall is well captured by the model with a high POD (96% for the range of 35.6–64.4 mm/day) and a good correlation (65–97%) for the majority of storms. Similarly, the Brier Score showed a value of 0.01, indicating the high performance of the model forecast for maximum surface winds. The Critical Successive Index was 0.6, indicating the moderate model performance in the prediction of tracks. It is evident from the statistical analysis that the performance of the model is good in forecasting storm structure, intensity and rainfall. However, the IMDAA data have certain limitations in predicting the tracks due to inadequate representation of the large-scale circulations, necessitating improvement. Full article
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<p>Study area map showing topography and the configured domains. The domains have horizontal resolutions of 12 km and 4 km, respectively.</p>
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<p>Climatological analysis of tropical cyclones over the Bay of Bengal (BoB) during 1982–2020, representing: (<b>a</b>) different categories of TCs and their frequency (CS: cyclonic storm, SCS: severe cyclonic storm, VSCS: very severe cyclonic storm, ESCS: extremely severe cyclonic storm, SUCS: super cyclonic storm), (<b>b</b>) genesis locations of ESCSs (Marked in Red), (<b>c</b>) hotspots of TCs genesis locations, (<b>d</b>) tracks of ESCSs, (<b>e</b>) rapid intensification of ESCSs (red ovals—Amphan, 18 May 2020 at 00UTC; Fani, 30 April 2019 at 03UTC; Hudhud, 11 October 2014 at 06UTC; Phailin, 10 October 2013 at 06UTC; Sidr, 13 November 2007 at 00UTC), and (<b>f</b>) trend analysis of ESCS duration and intensity (Source: [<a href="#B5-climate-13-00017" class="html-bibr">5</a>,<a href="#B22-climate-13-00017" class="html-bibr">22</a>]).</p>
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<p>Synoptic features in terms of atmospheric conditions and large-scale flows, including geopotential height (in contours), relative humidity (shaded), and wind vectors at 850 hPa from ERA5 analysis at 00 UTC during the life cycle of cyclonic storms: (<b>a1</b>–<b>a5</b>) Amphan; (<b>b1</b>–<b>b5</b>) Fani; (<b>c1</b>–<b>c5</b>) Hudhud; (<b>d1</b>–<b>d5</b>) Phailin; (<b>e1</b>–<b>e5</b>) Sidr.</p>
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<p>Initial low-pressure vortices of five ESCSs: (<b>a</b>) Amphan, (<b>b</b>) Fani, (<b>c</b>) Hudhud, (<b>d</b>) Phailin, and (<b>e</b>) Sidr—derived from the IMDAA dataset were compared with the IMD best-fit track data, indicating the location in the terms of the weather symbol.</p>
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<p>Model-simulated tracks of five ESCSs: (<b>a</b>) Amphan, (<b>b</b>) Fani, (<b>c</b>) Hudhud, (<b>d</b>) Phailin, and (<b>e</b>) Sidr along with IMD best-fit tracks.</p>
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<p>Temporal evaluation of along- and across-track errors for five ESCSs over the Bay of Bengal.</p>
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<p>Temporal variation in model-simulated MSW (in m/s), (<b>a</b>) Amphan, (<b>b</b>) Fani, (<b>c</b>) Hudhud, (<b>d</b>) Phailin, and (<b>e</b>) Sidr along with the IMD best-fit track dataset.</p>
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<p>Simulated wind fields (m/s) during intensification of ESCSs: (<b>a</b>) Amphan; (<b>b</b>) Fani; (<b>c</b>) Hudhud; (<b>d</b>) Phailin; and (<b>e</b>) Sidr.</p>
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<p>Simulated wind fields (m/s) before landfall of ESCSs: (<b>a</b>) Amphan; (<b>b</b>) Fani; (<b>c</b>) Hudhud; (<b>d</b>) Phailin; and (<b>e</b>) Sidr.</p>
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<p>Wind speed changes in 24 h (in m/s) for five ESCSs from model simulations and the IMD best-fit track dataset: (<b>a</b>) Amphan, (<b>b</b>) Fani, (<b>c</b>) Hudhud, (<b>d</b>) Phailin, and (<b>e</b>) Sidr.</p>
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<p>Temporal variation in model-simulated central sea level pressure (CSLP) for five ESCSs: (<b>a</b>) Amphan, (<b>b</b>) Fani, (<b>c</b>) Hudhud, (<b>d</b>) Phailin, and (<b>e</b>) Sidr, along with the IMD best-fit track dataset.</p>
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<p>Taylor diagrams of MSW (<b>a</b>–<b>e</b>) and CSLP (<b>f</b>–<b>j</b>) for five ESCSs [(<b>a</b>,<b>f</b>) Amphan, (<b>b</b>,<b>g</b>) Fani, (<b>c</b>,<b>h</b>) Hudhud, (<b>d</b>,<b>i</b>) Phailin and (<b>e</b>,<b>j</b>) Sidr].</p>
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<p>Accumulated rainfall (in mm/day) over 24 h for the five ESCSs presented as (<b>a</b>–<b>e</b>, <b>left</b> panel) model-simulated, and (<b>f</b>–<b>j</b>, <b>right</b> panel) TRMM rainfall data.</p>
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<p>Temperature anomaly for five ESCSs, namely (<b>a</b>) Amphan at 00 UTC on 19 May 2020, (<b>b</b>) Fani at 03 UTC on 2 May 2019, (<b>c</b>) Hudhud at 12 UTC on 11 October 2014, (<b>d</b>) Phailin at 12 UTC on 11 October 2013, and (<b>e</b>) Sidr at 03 UTC on 15 November 2007 obtained from model-forecasted (<b>left</b> panel) and compared with satellite observations (<b>f</b>–<b>j</b>, <b>right</b> panel), respectively.</p>
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<p>Simulated maximum reflectivity (in dBZ) for the Hudhud cyclone at (<b>a</b>) 1500 UTC, (<b>b</b>) 1800 UTC, and (<b>c</b>) 2100 UTC on 11 October 2014 (<b>a</b>–<b>c</b>) and are compared with the DWR images of Vishakhapatnam (<b>d</b>–<b>f</b>).</p>
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16 pages, 2665 KiB  
Article
Using Hybrid Deep Learning Models to Predict Dust Storm Pathways with Enhanced Accuracy
by Mahdis Yarmohamadi, Ali Asghar Alesheikh and Mohammad Sharif
Climate 2025, 13(1), 16; https://doi.org/10.3390/cli13010016 - 12 Jan 2025
Viewed by 633
Abstract
As a potential consequence of climate change, the intensity and frequency of dust storms are increasing. A dust storm arises when strong winds blow loose dust from a dry surface, transporting soil particles from one place to another. The environmental and human health [...] Read more.
As a potential consequence of climate change, the intensity and frequency of dust storms are increasing. A dust storm arises when strong winds blow loose dust from a dry surface, transporting soil particles from one place to another. The environmental and human health impacts of dust storms are substantial. Accordingly, studying the monitoring of this phenomenon and predicting its pathways for early decision making and warning are vital. This study employs deep learning methods to predict dust storm pathways. Specifically, hybrid CNN-LSTM and ConvLSTM models have been proposed for the 24 h-ahead prediction of dust storms in the region under study. The Modern-Era Retrospective Analysis for Research and Applications version 2 (MERRA-2) product that includes the dust particles and the meteorological information, such as surface wind speed and direction, relative humidity, surface air temperature, and skin temperature, is used to train the proposed models. These contextual features are selected utilizing the random forest feature importance method. The results indicate an improvement in the performance of both models by considering the contextual information. Moreover, a 0.2 increase in the Kappa coefficient criterion across all forecast hours indicates the CNN-LSTM model outperforms the ConvLSTM model when contextual information is considered. Full article
(This article belongs to the Special Issue Addressing Climate Change with Artificial Intelligence Methods)
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<p>Study region: West, Central, and South Asia.</p>
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<p>Architecture of proposed CNN-LSTM model.</p>
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<p>Architecture of proposed ConvLSTM model.</p>
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<p>Confusion matrix.</p>
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<p>Predicted and actual results for a sample dust storm using the CNN-LSTM method at t, t + 6, t + 12, t + 18, and t + 24.</p>
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<p>Predicted and actual results for a sample dust storm using ConvLSTM at t, t + 6, t + 12, t + 18, and t + 24.</p>
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26 pages, 9938 KiB  
Article
Correlating Fire Incidents with Meteorological Variables in Dry Temperate Forest
by Khurram Abbas, Ali Ahmed Souane, Hasham Ahmad, Francesca Suita, Zhan Shu, Hui Huang and Feng Wang
Forests 2025, 16(1), 122; https://doi.org/10.3390/f16010122 - 10 Jan 2025
Viewed by 393
Abstract
Forest fires pose a significant ecological threat, particularly in the Diamer District, Gilgit-Baltistan, Pakistan, where climatic factors combined with human activities have resulted in severe fire incidents. The present study sought to investigate the correlation between the incidence of forest fires and critical [...] Read more.
Forest fires pose a significant ecological threat, particularly in the Diamer District, Gilgit-Baltistan, Pakistan, where climatic factors combined with human activities have resulted in severe fire incidents. The present study sought to investigate the correlation between the incidence of forest fires and critical meteorological elements, including temperature, humidity, precipitation, and wind speed, over a period of 25 years, from 1998 to 2023. We analyzed 169 recorded fire events, collectively burning approximately 109,400 hectares of forest land. Employing sophisticated machine learning algorithms, Random Forest (RF), and Gradient Boosting Machine (GBM) revealed that temperature and relative humidity during the critical fire season, which spans May through July, are key factors influencing fire activity. Conversely, wind speed was found to have a negligible impact. The RF model demonstrated superior predictive accuracy compared to the GBM model, achieving an RMSE of 5803.69 and accounting for 49.47% of the variance in the burned area. This study presents a novel methodology for predictive fire risk modeling under climate change scenarios in the region, offering significant insights into fire management strategies. Our results underscore the necessity for real-time early warning systems and adaptive management strategies to mitigate the frequency and intensity of escalating forest fires driven by climate change. Full article
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<p>Map of Diamer District, Gilgit-Baltistan.</p>
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<p>(<b>a</b>) Digital elevation model value, (<b>b</b>) hill shade value, (<b>c</b>) aspect value, and (<b>d</b>) slope value.</p>
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<p>(<b>a</b>) Diamer district’s annual burned area of forest fires, 1998–2023; (<b>b</b>) Diamer District’s annual forest fire occurrence of different causes from 1998 to 2023.</p>
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<p>(<b>a</b>) Diamer District, Julian dates of fires from 1998 to 2023; (<b>b</b>) Diamer District, Julian dates of huge fires from 1998 to 2023.</p>
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<p>Julian dates of the earliest and latest forest fires in the Diamer District from 1998 to 2023. blue bullets and line signifies early fire events and its regression, red bullets and line shows later fire events and its regression.</p>
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<p>Diamer District, annual climate conditions in May, June, and July from 1998 to 2023. (<b>a</b>) temperature; (<b>b</b>) relative humidity; (<b>c</b>) annual rainfall; (<b>d</b>) wind speed.</p>
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<p>Climate–fire relationships in the Diamer District from 1998 to 2023. (<b>a</b>) temperature; (<b>b</b>) relative humidity; (<b>c</b>) rainfall; (<b>d</b>) wind speed. bullets, lines, and shadows represents fire events, regression and correlation, respectively.</p>
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<p>Climate–fire relationships in the Diamer District in May from 1998 to 2023. (<b>a</b>) temperature; (<b>b</b>) relative humidity; (<b>c</b>) rainfall; (<b>d</b>) wind speed.</p>
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<p>Squared error loss across iterations for random forest and GBM models. The black curve is training set loss and the green and red curves represent validation loss for the Random Forest and Gradient Boosting Machine models, respectively. The blue dashed line represents the optimal point of iteration for the Gradient Boosting Machine model. The figure represents the model’s learning dynamics: Random Forest depicts a relatively low overall error with more stable convergence compared to Gradient Boosting Machine, showing a growing error from overfitting at the later iterations.</p>
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<p>Feature importance plot for Random Forest.</p>
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<p>Variable importance in the Gradient Boosting Model (GBM). The x-axis is the relative influence of each variable on a scale from 0 to 100%. The higher the value, the more significantly the variable contributes to the model’s predictions. In this figure, ‘forest_fire_alarms’ is the most important variable, contributing almost entirely to the prediction, while ‘MEAN_ELEVATION’ shows negligible influence.</p>
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<p>Residuals (predicted—actual burned area) for the Random Forest Model, illustrating that the x-axis shows the actual burned area (in hectares), while the y-axis indicates the residuals. The point that is closer to the red dashed line at 0 indicates better predictions. Negative residuals suggest the model tends to underestimate, especially for larger burned areas. Additional analysis suggests potential bias in the model’s handling of larger fire events.</p>
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<p>Residuals (predicted—actual burned area) for the Gradient Boosting Model (GBM), showing the actual burned area (in hectares) on the x-axis, while residuals are on the y-axis. Points closer to the red dashed line suggest better predictions. Larger residuals, particularly for larger burned areas, suggest the model underestimates burn areas, similar to the Random Forest model. This pattern reflects the challenges of accurately predicting extreme fire events using the GBM.</p>
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<p>Partial Dependence Plot (PDP) for the Log of Burned Area in the Random Forest Model, showing the log-transformed burned area (in hectares) on the x-axis, while indicating the predicted burned area on the y-axis. The plot suggests that for low log burned area values (below 3), the predicted area remains stable at around 3000 hectares. However, predictions increase sharply when the log burned area exceeds, highlighting that the model predicts significantly higher burned areas for larger fires, suggesting the model’s sensitivity to extreme fire events.</p>
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<p>Partial Dependence Plot (PDP) for the Log of Burned Area in the Gradient Boosting Model (GBM).</p>
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<p>Correlation heatmap of fire metrics, including meteorological and environmental factors. It shows the interrelation between different fire metrics and the environmental parameters of precipitation, temperature, and relative humidity.</p>
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12 pages, 2168 KiB  
Article
Optimization of Fused Deposition Modeling Parameters for Mechanical Properties of Polylactic Acid Parts Based on Kriging and Cuckoo Search
by Yuan Yang, Yiyang Wang, Bowen Xue, Changxu Wang and Bo Yang
Aerospace 2025, 12(1), 38; https://doi.org/10.3390/aerospace12010038 - 10 Jan 2025
Viewed by 323
Abstract
As an emerging rapid manufacturing technology, 3D printing has been widely applied in numerous fields such as aerospace, shipbuilding, and wind power, by virtue of its advantage in efficiently fabricating components with complex structures and integrated functions. In response to the problems of [...] Read more.
As an emerging rapid manufacturing technology, 3D printing has been widely applied in numerous fields such as aerospace, shipbuilding, and wind power, by virtue of its advantage in efficiently fabricating components with complex structures and integrated functions. In response to the problems of poor mechanical properties and difficulty in selecting process parameters for fused deposition modeling (FDM), this paper analyzed the principle of FDM and proposed a parameter optimization method based on a Kriging and Cuckoo Search (CS) algorithm aimed at improving the mechanical properties of 3D printed polylactic acid (PLA) parts. Firstly, by analyzing FDM principle and its main parameters, printing speed and temperature were selected as research elements, and tensile strength as the mechanical performance index. Latin hypercube sampling (LHS) was integrated to generate a limited experimental sample set. Secondly, a Kriging-based prediction model for mechanical properties was constructed by learning sample data, and the nonlinear mapping relationship between process parameters and tensile strength was obtained. Then, using the combinations of speed and temperature as design variables and maximizing tensile strength as the optimization objective, an optimization model was established, and the optimal process parameters were searched by CS. The optimal printing velocity was 31 mm/s and printing temperature was 225 °C, and the corresponding maximum tensile strength was 38.27 MPa. Finally, compared to the test data, the relative prediction error of Kriging model was 0.62%, and the optimal strength (38.27 MPa) increased by about 12.7% compared to the average value (33.97 MPa) of experimental data. It can be seen that the Kriging model is effective, and the tensile strength of parts printed under the optimal process parameters is significantly improved. Full article
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<p>FDM printing principle.</p>
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<p>Flow chart for optimizing FDM process parameters based on Kriging and CS.</p>
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<p>Dog-bone-shaped specimens and dimensions.</p>
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<p>Tensile test.</p>
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<p>PLA specimens after tension.</p>
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<p>Kriging response surface.</p>
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<p>The predicted and expected values of Kriging.</p>
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<p>Convergence curve of tensile strength by CS.</p>
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19 pages, 1296 KiB  
Article
MIESTC: A Multivariable Spatio-Temporal Model for Accurate Short-Term Wind Speed Forecasting
by Shaohan Li, Min Chen, Lu Yi, Qifeng Lu and Hao Yang
Atmosphere 2025, 16(1), 67; https://doi.org/10.3390/atmos16010067 - 9 Jan 2025
Viewed by 272
Abstract
Wind speed forecasting is an essential part of weather prediction, with significant value in economics, business, and management. Utilizing multiple meteorological variables can improve prediction accuracy, but existing methods face challenges such as mixing and noise due to variable differences, as well as [...] Read more.
Wind speed forecasting is an essential part of weather prediction, with significant value in economics, business, and management. Utilizing multiple meteorological variables can improve prediction accuracy, but existing methods face challenges such as mixing and noise due to variable differences, as well as difficulty in capturing complex spatio-temporal dependencies. To address these issues, this study introduces a novel short-term wind speed forecasting model named as MIESTC. The proposed model employs an independent encoder to extract features from each meteorological variable, mitigating the issues of noise that are caused by variable mixing. Then, a multivariate spatio-temporal correlation module is used to capture the global spatio-temporal dependencies between variables and model their interactions. Experimental results on the ERA5-LAND dataset show that, compared to the ConvLSTM, UNET, and SimVP models, the MIESTC model reduces RMSE by 14.60%, 8.64%, and 10.41%, respectively, for a 1 h prediction duration. For a 6 h prediction duration, the corresponding reductions are 13.91%, 8.20%, and 6.95%, validating its superior performance in short-term wind speed forecasting. Furthermore, an analysis of variable impacts reveals that U10, V10, and T2M play dominant roles in wind speed prediction, while TP exhibits a relatively lower impact, aligning with the results of the correlation analysis. These findings underscore the potential of MIESTC as an effective and reliable tool for short-term wind speed prediction. Full article
(This article belongs to the Special Issue Applications of Artificial Intelligence in Atmospheric Sciences)
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<p>Research area and five research sites.</p>
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<p>Correlation analysis of different factors with wind speed across five locations. A, B, C, D, and E represent the five research locations in the study. The chart shows that the correlation between the wind speed and various factors differs significantly across locations. The factors u10, v10, and t2m exhibit strong correlations with the wind speed at multiple locations, suggesting their importance as primary influencing factors, whereas sp and tp show relatively strong correlations at specific locations.</p>
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<p>An overview of the MIESTC model’s architecture. Subfigure (<b>a</b>) illustrates the overall workflow, including the independent encoding of multiple meteorological variables (WS, U10, V10, T2M, TP, SP), spatio-temporal feature extraction through the MSTC module to capture the spatio-temporal relationships between variables, and finally the decoding and prediction using the predictor module. The skip connection aids in preserving features from earlier stages. Subfigures (<b>b</b>–<b>d</b>) present the detailed structures of the encoder block, MSTC block, and predictor block.</p>
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<p>The data distribution of the meteorological variables. These variables clearly exhibit significant differences in their distributions, with distinct scales and semantic units.</p>
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<p>Model performance comparison. This figure presents the performances of various models at different prediction time horizons, evaluated with RMSE, PCC, MAE, and SSIM metrics. The results indicate that the MIESTC model consistently surpasses other models across all time steps and evaluation metrics, highlighting its superior effectiveness in short-term wind speed forecasting.</p>
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<p>Visual representation of wind speed prediction results across different models. The red boxes indicate areas where the prediction deviates significantly from the ground truth, highlighting the deficiencies in different models.</p>
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<p>Attention weight distribution of wind speed prediction variables. This heatmap illustrates the attention weight distribution of each meteorological variable (U10, V10, T2M, SP, TP, WS) across eight attention heads in the MSTC module. The attention heads (Head 1 to Head 8) represent different perspectives of the model in capturing variable relationships. Darker colors indicate higher attention weights, highlighting the relative importance of each variable for wind speed prediction.</p>
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21 pages, 9857 KiB  
Article
Short- to Medium-Term Weather Forecast Skill of the AI-Based Pangu-Weather Model Using Automatic Weather Stations in China
by Siyi Xu, Yize Zhang, Junping Chen and Yunlong Zhang
Remote Sens. 2025, 17(2), 191; https://doi.org/10.3390/rs17020191 - 8 Jan 2025
Viewed by 428
Abstract
Pangu is an AI-based model designed for rapid and accurate numerical weather forecasting. To evaluate Pangu’s short- to medium-term weather forecasting skill over various meteorological parameters, this paper validated its performance in predicting temperature, wind speed, wind direction, and barometric pressure using data [...] Read more.
Pangu is an AI-based model designed for rapid and accurate numerical weather forecasting. To evaluate Pangu’s short- to medium-term weather forecasting skill over various meteorological parameters, this paper validated its performance in predicting temperature, wind speed, wind direction, and barometric pressure using data from over 2000 weather stations in China. Pangu’s performance was compared with ECMWF-HRES and GFS to assess its effectiveness relative to traditional high-precision NWP models under real meteorological conditions. Furthermore, the more recent FuXi and FengWu models were included in the analysis to further validate Pangu’s forecasting skill. The study examined Pangu’s forecast performance from spatial perspectives, evaluated the dispersion of forecast deviations, and analyzed its performance at different lead times and with various initial fields. The iteration precision of Pangu’s four forecast models with lead times of 1 h, 3 h, 6 h, and 24 h was also assessed. Finally, a case study on typhoon track forecasting was conducted to evaluate Pangu’s performance in predicting typhoon paths. The results indicate that Pangu surpasses traditional NWP systems in temperature forecasting, while its performance in predicting wind direction, wind speed and pressure is comparable to them. Additionally, the forecast skill of Pangu diminishes as the lead time extends, but it tends to surpass traditional NWP systems with longer lead times. Moreover, FuXi and FengWu demonstrate even higher accuracy compared to Pangu. Pangu’s performance is also dependent on initial fields, and the temperature forecasting of Pangu is more sensitive to the initial field compared with other meteorological parameters. Furthermore, the iteration precision of Pangu’s 1 h forecast model is significantly lower than that of the other models, but this discrepancy in precision may not be prominently reflected in Pangu’s actual forecasting process due to the greedy algorithm employed. In the case study on typhoon forecasting, Pangu, along with FuXi and FengWu, demonstrates comparable performance in predicting Bebinca’s track compared to ECMWF and outperforms GFS in its track predictions. This study demonstrated Pangu’s applicability in short- to medium-term forecasting of meteorological parameters, showcasing the significant potential of AI-based numerical weather models in enhancing forecast performance. Full article
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<p>Distribution of regional weather stations in China.</p>
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<p>The selected time (where rows represent dates, and columns represent daily timepoints) and frequency of usage of the initial field for ECMWF (<b>a</b>), GFS and Pangu (<b>b</b>).</p>
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<p>Temperature forecast mean bias map by Pangu (<b>a</b>), ECMWF (<b>b</b>), and GFS (<b>c</b>) for all days from 30 October to 5 November 2023.</p>
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<p>Pressure forecast mean bias map by Pangu (<b>a</b>), ECMWF (<b>b</b>), and GFS (<b>c</b>) for all days from 30 October to 5 November 2023.</p>
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<p>Wind rose of Pangu (<b>a</b>), ECMWF (<b>b</b>), GFS (<b>c</b>) and the observed values (<b>d</b>).</p>
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<p>The 3 h to 16-day MAE (left) and RMSE (right) of temperature (<b>a</b>), wind speed (<b>b</b>), wind direction (<b>c</b>), and pressure (<b>d</b>) forecasted by Pangu, ECMWF, GFS, FuXi, and FengWu, along with their 90% confidence intervals.</p>
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<p>The 3 h to 16-day MAE (left) and RMSE (right) of temperature (<b>a</b>), wind speed (<b>b</b>), wind direction (<b>c</b>), and pressure (<b>d</b>) forecasted by Pangu, ECMWF, GFS, FuXi, and FengWu, along with their 90% confidence intervals.</p>
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<p>MAE and RMSE of temperature (<b>a</b>), wind speed (<b>b</b>), wind direction (<b>c</b>), and pressure (<b>d</b>) forecasted by Pangu using ERA5 and GFS as the initial field, with the 90% confidence intervals displayed as black vertical error bars.</p>
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<p>ACC with 90% confidence intervals of temperature (<b>a</b>), wind speed (<b>b</b>), wind direction (<b>c</b>), and pressure (<b>d</b>) forecasted by ERA5-initialized Pangu, GFS-initialized Pangu, ECMWF, and GFS, respectively.</p>
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<p>MAE and RMSE of Pangu’s forecasts for temperature (<b>a</b>), wind speed (<b>b</b>), wind direction (<b>c</b>), and pressure (<b>d</b>), with 90% confidence intervals on 30 October at 12:00 UTC, using 1 h, 3 h, 6 h, and 24 h forecast models.</p>
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<p>MAE and RMSE of Pangu’s forecasts for temperature (<b>a</b>), wind speed (<b>b</b>), wind direction (<b>c</b>), and pressure (<b>d</b>), with 90% confidence intervals on 30 October at 12:00 UTC, using 1 h, 3 h, 6 h, and 24 h forecast models.</p>
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<p>Track forecast for typhoon Bebinca, based on initial conditions from 13 September 2024 at 12:00 UTC.</p>
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<p>Intermediate results for tracking Typhoon Bebinca on 16 September 2024 at 06:00 UTC: (<b>a</b>) ERA5 reanalysis data, (<b>b</b>) ECMWF forecast, (<b>c</b>) Pangu forecast, (<b>d</b>) FuXi forecast.</p>
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32 pages, 10088 KiB  
Article
Fast Simulation of the Flow Field in a VAWT Wind Farm Using the Numerical Data Obtained by CFD Analysis for a Single Rotor
by Yutaka Hara, Md. Shameem Moral, Aoi Ide and Yoshifumi Jodai
Energies 2025, 18(1), 220; https://doi.org/10.3390/en18010220 - 6 Jan 2025
Viewed by 429
Abstract
The effects of an increase in output power owing to the close arrangement of vertical-axis wind turbines (VAWTs) are well known. With the ultimate goal of determining the optimal layout of a wind farm (WF) for VAWTs, this study proposes a new method [...] Read more.
The effects of an increase in output power owing to the close arrangement of vertical-axis wind turbines (VAWTs) are well known. With the ultimate goal of determining the optimal layout of a wind farm (WF) for VAWTs, this study proposes a new method for quickly calculating the flow field and power output of a virtual WF consisting of two-dimensional (2-D) miniature VAWT rotors. This new method constructs a flow field in a WF by superposing 2-D velocity numerical data around an isolated single VAWT obtained through a computational fluid dynamics (CFD) analysis. In the calculation process, the VAWTs were gradually increased one by one from the upstream side, and a calculation subroutine, in which the virtual upstream wind speed at each VAWT position was recalculated with the effects of other VAWTs, was repeated three times for each arrangement with a temporal number of VAWTs. This method includes the effects of the velocity gradient, secondary flow, and wake shift as models of turbine-to-turbine interaction. To verify the accuracy of the method, the VAWT rotor power outputs predicted by the proposed method for several types of rotor pairs, four-rotor tandem, and parallel arrangements were compared with the results of previous CFD analyses. This method was applied to four virtual WFs consisting of 16 miniature VAWTs. It was found that a layout consisting of two linear arrays of eight closely spaced VAWTs with wide spacing between the arrays yielded a significantly higher output than the other three layouts. The high-performance layout had fewer rotors in the wakes of the other rotors, and the induced flow speeds generated by the closely spaced VAWTs probably mutually enhanced their output power. Full article
(This article belongs to the Section A3: Wind, Wave and Tidal Energy)
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<p>The proposed method for simulating a VAWT wind farm using the numerical velocity data obtained by CFD analysis for a single isolated rotor.</p>
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<p>Extrapolation regions [A] to [H].</p>
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<p>The effects of velocity gradient <span class="html-italic">du</span>/<span class="html-italic">dy</span> and secondary component <span class="html-italic">v</span> on wind turbine rotor power. In the figure, the red arrows indicate the direction of rotation of the wind turbine rotor, and the green arrow indicates the velocity vector of the inflow wind (the combination of <span class="html-italic">u</span> and <span class="html-italic">v</span> components).</p>
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<p>(<b>a</b>) Three typical arrangements of VAWT–rotor pairs. (<b>b</b>) The effects of rotor solidity on the normalized average power of a rotor pair.</p>
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<p>The assumed rotor performance (power and rotational speed) of a miniature rotor, which is based on CFD results obtained at wind speed of 10 m/s.</p>
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<p>Main calculation process: (<b>a</b>) <span class="html-italic">N</span><sub>temp</sub> = 1; (<b>b</b>) <span class="html-italic">N</span><sub>temp</sub> = 2; (<b>c</b>) <span class="html-italic">N</span><sub>temp</sub> = 3; (<b>d</b>) <span class="html-italic">N</span> = 4.</p>
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<p>The sub-calculation process (repetition) in the case of temporary rotor number <span class="html-italic">N</span><sub>temp</sub> = 3: (<b>a</b>) Situation 1 (R1 is removed to calculate the revised <span class="html-italic">U</span><sub>F</sub>(1)). (<b>b</b>) Situation 2 (R2 is removed to calculate the revised <span class="html-italic">U</span><sub>F</sub>(2)). (<b>c</b>) Situation 3 (R3 is removed to calculate the revised <span class="html-italic">U</span><sub>F</sub>(3)).</p>
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<p>A comparison between the new model and CFD in the case of CO–25 mm. (<b>a</b>) A flow field for <span class="html-italic">θ</span> = 22.5°; (<b>b</b>) a flow field for <span class="html-italic">θ</span> = 337.5° (−22.5°); (<b>c</b>) the 16-wind-direction distribution of power of R1; (<b>d</b>) the 16-wind-direction distribution of averaged power of R1 and R2.</p>
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<p>A comparison between the new model and CFD in the case of IR–25 mm. (<b>a</b>) A flow field for <span class="html-italic">θ</span> = 0° (CD condition); (<b>b</b>) a flow field for <span class="html-italic">θ</span> = 180° (CU condition); (<b>c</b>) the 16-wind-direction distribution of power of R1; (<b>d</b>) the 16-wind-direction distribution of averaged power of R1 and R2.</p>
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<p>(<b>a</b>) Normalized power difference in R1 (<span class="html-italic">Err</span><sub>n_R1</sub>) between CFD and present model predictions. (<b>b</b>) Normalized average power difference in R1 and R2 (<span class="html-italic">Err</span><sub>n_ave</sub>) between CFD and present model predictions (grid number: <span class="html-italic">m</span> = 400. Colors show the difference in normalized cell size: <span class="html-italic">Cell</span><sub>n_D</sub> = 0.05, 0.1, 0.2, 0.4, 0.75).</p>
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<p>(<b>a</b>) Normalized power difference in R1 (<span class="html-italic">Err</span><sub>n_R1</sub>) between CFD and present model predictions. (<b>b</b>) Normalized average power difference in R1 and R2 (<span class="html-italic">Err</span><sub>n_ave</sub>) between CFD and present model predictions (grid number: <span class="html-italic">m</span> = 600. Colors show the difference in normalized cell size: <span class="html-italic">Cell</span><sub>n_D</sub> = 0.0333, 0.0667, 0.1333, 0.2667, 0.5).</p>
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<p>A comparison of the power prediction between (<b>a</b>) CFD (unsteady) and the (<b>b</b>) present model (steady) in the case of a four-VAWT parallel arrangement (unit of power: mW).</p>
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<p>A comparison of the power prediction between (<b>a</b>) CFD (unsteady) and the (<b>b</b>) present model (steady) in the case of a four-VAWT tandem arrangement (unit of power: mW).</p>
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<p>(<b>a</b>) The flow field and output power of each turbine at <span class="html-italic">θ</span> = 0° in the CO–4 × 4 layout. (<b>b</b>) The wind-direction dependence of the averaged power of 16 VAWTs.</p>
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<p>(<b>a</b>) The flow field and output power of each turbine at <span class="html-italic">θ</span> = 0° in the CO–8–pairs layout. (<b>b</b>) The wind-direction dependence of the averaged power of 16 VAWTs.</p>
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<p>(<b>a</b>) The flow field and output power of each turbine at <span class="html-italic">θ</span> = 0° in the IR–8–pairs layout. (<b>b</b>) The wind-direction dependence of the averaged power of 16 VAWTs.</p>
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<p>(<b>a</b>) The flow field and output power of each turbine at <span class="html-italic">θ</span> = 0° in the CO–8 × 2 layout. (<b>b</b>) The wind-direction dependence of the averaged power of 16 VAWTs.</p>
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<p>The nonuniform wind direction probability (<span class="html-italic">WDP</span>) distribution observed in the Arid Land Research Center of Tottori University. Wind-direction angle <span class="html-italic">θ<sub>i</sub></span> = 0 corresponds to the north in this figure.</p>
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<p>(<b>a</b>) A 3-D model of a miniature butterfly wind turbine. (<b>b</b>) The 2-D rotor used for 2-D CFD analysis.</p>
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<p>The mesh conditions for CFD analysis to investigate the torque performance of a single rotor.</p>
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<p>An example of the unsteady flow field around a single rotor obtained by CFD analysis.</p>
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<p>The torque performance of a miniature rotor (S-size) obtained by CFD analysis and an ideal load torque curve defined by Equation (A1).</p>
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<p>Three 2-D rotors with different solidities. (<b>a</b>) M size; (<b>b</b>) ML size; and (<b>c</b>) L size.</p>
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<p>The mesh near a rotor pair arranged as the CD layout (M-size, <span class="html-italic">gap</span> = 0.2<span class="html-italic">D</span>).</p>
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<p>Distributions of <span class="html-italic">x</span>-direction component (<span class="html-italic">u</span>) of flow velocity of CO-arrangement in each rotor pair case. (<b>a</b>) S size; (<b>b</b>) M size; (<b>c</b>) ML size; and (<b>d</b>) L size.</p>
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<p>Variation in angular velocity and torque of each rotor (R1, R2) of ML size in CO arrangement. (<b>a</b>) <span class="html-italic">t</span> = 0 to 25 s, (<b>b</b>) <span class="html-italic">t</span> = 23 to 25 s (partial expansion of (<b>a</b>)).</p>
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<p>Variation in mechanical power (product of <span class="html-italic">ω</span> and <span class="html-italic">Q</span>) of each rotor (R1 and R2) of ML size in CO arrangement. (<b>a</b>) <span class="html-italic">t</span> = 0 to 25 s, (<b>b</b>) <span class="html-italic">t</span> = 23 to 25 s (partial expansion of (<b>a</b>)).</p>
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17 pages, 1703 KiB  
Article
Refined Assessment Method of Offshore Wind Resources Based on Interpolation Method
by Wenchuan Meng, Zaimin Yang, Zhi Rao, Shuang Li, Xin Lin, Jingkang Peng, Yuwei Cao and Yingquan Chen
Energies 2025, 18(1), 213; https://doi.org/10.3390/en18010213 - 6 Jan 2025
Viewed by 336
Abstract
To enhance the prediction accuracy of offshore wind speed, this study employs an interpolation algorithm to improve spatial resolution based on the ERA5 reanalysis dataset. The objective is to identify the optimal interpolation method and apply it to wind energy assessments in the [...] Read more.
To enhance the prediction accuracy of offshore wind speed, this study employs an interpolation algorithm to improve spatial resolution based on the ERA5 reanalysis dataset. The objective is to identify the optimal interpolation method and apply it to wind energy assessments in the South China Sea. This paper compares the interpolation effects and accuracy of Linear, Cubic, and Bicubic interpolation methods on wind speed data, with the optimal method subsequently applied to evaluate wind resources in the South China Sea for 2023. The findings indicate that, while different interpolation methods minimally affect the correlation of wind speed data, there are notable differences in their impact on overall accuracy. The Cubic interpolation method proved to be the most effective, tripling spatial resolution and reducing wind speed errors in ERA5 data by 26%. Using this method, wind resource assessments were conducted in selected areas of the South China Sea. Results reveal that the annual available operational hours for wind turbines in most parts of the region range from 2000 to 4000 h, with fluctuations in turbine output power increasing alongside available operational hours. Full article
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<p>Changes in wind speed at different stations before and after interpolation: (<b>a</b>–<b>c</b>) (22101) and (<b>d</b>–<b>f</b>) (22103).</p>
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<p>Changes in wind speed at different stations before and after interpolation: (<b>a</b>–<b>c</b>) (22104) and (<b>d</b>–<b>f</b>) (22105).</p>
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<p>Changes in wind speed at different stations before and after interpolation: (<b>a</b>–<b>c</b>) (22107) and (<b>d</b>–<b>f</b>) (22108).</p>
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<p>Effect of Cubic interpolation.</p>
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<p>Power curve of 8 MW wind turbine.</p>
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<p>Annual availability hours of different sub-regions in the South China Sea.</p>
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<p>Distribution of available hours in the South China Sea region.</p>
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<p>Relationship between available hours and wind turbine output volatility.</p>
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<p>Changes in wind speed in different sub-regions.</p>
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<p>Annual output power curve of Max region after storage.</p>
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<p>Annual output power curve of the Median area after storage allocation.</p>
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26 pages, 10210 KiB  
Article
Research on the Simulation Model of Dynamic Shape for Forest Fire Burned Area Based on Grid Paths from Satellite Remote Sensing Images
by Xintao Ling, Gui Zhang, Ying Zheng, Huashun Xiao, Yongke Yang, Fang Zhou and Xin Wu
Remote Sens. 2025, 17(1), 140; https://doi.org/10.3390/rs17010140 - 3 Jan 2025
Viewed by 371
Abstract
The formation of forest fire burned area, influenced by a variety of factors such as meteorology, topography, vegetation, and human intervention, is a dynamic process of fire line burning that develops from the point of ignition to the boundary of the burned area. [...] Read more.
The formation of forest fire burned area, influenced by a variety of factors such as meteorology, topography, vegetation, and human intervention, is a dynamic process of fire line burning that develops from the point of ignition to the boundary of the burned area. Accurately simulating and predicting this dynamic process can provide a scientific basis for forest fire control and suppression decisions. In this study, five typical forest fires located in different regions of China were used as the study object. The straight path distances from the ignition point grid to each grid on fire line in Sentinel-2 imageries for each forest fire were used as the target variables. We obtained the values of 11 independent variables for each pathway, including wind speed component, Temperature, Relative Humidity, Elevation, Slope, Aspect, Degree of Relief, Normalized Difference Vegetation Index, Vegetation Type, Fire Duration, and Gross Domestic Product reflecting human intervention capacity for fires. The value of each target variable and that of its corresponding independent variable constituted a sample. Four machine learning models, such as Random Forest (RF), Gradient Boosting Decision Trees (GBDT), Support Vector Machine (SVM), and Multilayer Perceptron (MLP), were trained using 80% effective samples from four forest fires, and 20% used to verify the above models. The hyper-parameters of each model were optimized using grid search method. After analyzing the validation results of models which showed temperature as a non-significant variable, the training and validation process of models above was repeated after excluding temperature. The results show that RF is the optimal model with 49.55 m for root mean square error (RMSE), 29.19 m for mean absolute error (MAE) and 0.9823 for coefficient of determination (R2). This study used the RF model to construct the shape of burned areas by predicting lengths of all straight path distances from the ignition point to the fire line. The study can dynamically capture the development of forest fire scenes. Full article
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<p>Location of five typical forest fires in China.</p>
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<p>The technical route of this study.</p>
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<p>Simple schematics of four machine learning methods.</p>
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<p>The straight path in the forest fire area.</p>
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<p>The interrelationship diagram of <math display="inline"><semantics> <mrow> <mi>φ</mi> </mrow> </semantics></math>,<math display="inline"><semantics> <mrow> <mi>ϕ</mi> </mrow> </semantics></math>,<math display="inline"><semantics> <mrow> <mi>θ</mi> </mrow> </semantics></math>.</p>
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<p>The number of grids on a straight path from the ignition point to the fire line.</p>
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<p>Removes the special straight path.</p>
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<p>ROC curves prediction rates of four models.</p>
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<p>Extraction results of burned areas of five forest fires. (<b>a</b>–<b>d</b>) show the results of the burned area extraction for “Qinyuan 3.29” at two time points (2019-04-01 03:27 and 2019-04-04 05:00). (<b>e</b>–<b>h</b>) illustrate the results of the burned area extraction for “Gaoming 12.5” at two time points (2019-12-06 03:11 and 2019-12-08 10:30). (<b>i</b>–<b>l</b>) display the results of the burned area extraction for “Beibei 8.21” at two time points (2022-10-19 03:20 and 2022-08-26 00:30). (<b>m</b>–<b>p</b>) present the results of the burned area extraction for “Xintian 10.17” at two time points (2022-10-19 03:20 and 2022-10-26 13:00). Finally, (<b>q</b>–<b>t</b>) represent the results of the burned area extraction for “Muli 3.28” at two time points (2020-03-30 04:00 and 2020-04-08 09:00).</p>
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<p>The weight distribution of the independent variables of the four machine learning models.</p>
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<p>The scatter comparison between the predicted distance and the real distance of the four machine learning models.</p>
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<p>The residual error comparison of four machine learning models.</p>
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<p>Simulation results of the fire line for four forest fires using RF. (<b>a</b>,<b>b</b>) show the fire line simulation results for “Qinyuan 3.29” at two time points (2019-04-01 03:27 and 2019-04-04 05:00). (<b>c</b>,<b>d</b>) illustrate the fire line simulation results for “Gaoming 12.5” at two time points (2019-12-06 03:11 and 2019-12-08 10:30). (<b>e</b>,<b>f</b>) display the fire line simulation results for “Beibei 8.21” at two time points (2022-10-19 03:20 and 2022-08-26 00:30). Finally, (<b>g</b>,<b>h</b>) present the fire line simulation results for “Xintian 10.17” at two time points (2022-10-19 03:20 and 2022-10-26 13:00).</p>
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<p>The comparison of the simulated fire line and the real fire line for the “Muli 3.28” forest fire is shown. (<b>a</b>,<b>b</b>) represent the fire line simulation results for “Muli 3.28” at two time points (2020-03-30 04:00 and 2020-04-08 09:00).</p>
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21 pages, 18920 KiB  
Article
A Feasibility Analysis of Wind Energy Potential and Seasonal Forecasting Trends in Thatta District: A Project to Combat the Energy Crisis in Pakistan
by Jahangeer Khan Bhutto, Zhijun Tong, Tayyab Raza Fraz, Mazhar Baloch, Haider Ali, Jiquan Zhang, Xingpeng Liu and Yousef A. Al-Masnay
Energies 2025, 18(1), 158; https://doi.org/10.3390/en18010158 - 3 Jan 2025
Viewed by 602
Abstract
Wind energy has emerged as a viable alternative to fossil fuels due to its clean and cost-effective nature. Pakistan, facing growing energy demands and the imperative to reduce carbon emissions, has invested significantly in wind power to supply electric power in rural and [...] Read more.
Wind energy has emerged as a viable alternative to fossil fuels due to its clean and cost-effective nature. Pakistan, facing growing energy demands and the imperative to reduce carbon emissions, has invested significantly in wind power to supply electric power in rural and urban communities, particularly in the Thatta district of Sindh Province of Pakistan. However, the sustainability of wind energy generation is contingent upon consistent and sufficient wind resources. This study examines the wind potential of Thatta district from 2004 to 2023 to assess its suitability for large-scale wind power development. To evaluate the wind potential of Thatta district, seasonal wind speed and direction data were collected and analyzed. Wind shear at different heights was determined using the power law, and wind potential maps were generated using GIS interpolation techniques. Betz’s law was employed to assess wind turbine power density. Box–Jenkins ARIMA and SARIMA models were applied to predict future wind patterns. This study revealed that Thatta district experienced sufficient wind speeds during the study period, with averages of 9.7 m/s, 7.6 m/s, 7.4 m/s, and 4.8 m/s for summer, autumn, spring, and winter, respectively. However, a concerning trend of decreasing wind speeds has been observed since 2009. The most significant reductions occurred in summer, coinciding with Pakistan’s peak electricity demand. While Thatta district has historically demonstrated potential for wind energy, the declining wind speeds pose a challenge to the sustainability of wind power projects. Further research is necessary to identify the causes of this trend and to explore mitigation strategies. Full article
(This article belongs to the Section A3: Wind, Wave and Tidal Energy)
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<p>(<b>a</b>) Total cumulative installed capacity, (<b>b</b>) new capacity, (<b>c</b>) growth rates, and (<b>d</b>) wind power capacity by country [<a href="#B7-energies-18-00158" class="html-bibr">7</a>].</p>
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<p>Average wind velocity in different provinces of Pakistan.</p>
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<p>Spatial variation in wind velocity in Sindh province of Pakistan.</p>
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<p>Study area location.</p>
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<p>(<b>a</b>) Study area and its adjacent districts. (<b>b</b>) The exact location of wind power plants in Thatta, Sindh, Pakistan.</p>
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<p>Illustration of spatiotemporal variation in average wind speed and direction calculated at (50 m) during summer (2004–2023).</p>
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<p>Illustration of spatiotemporal variation in average wind speed and direction calculated at (50 m) during summer (2004–2023).</p>
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<p>Illustration of spatiotemporal variation in average wind speed and direction calculated at (50 m) during autumn (2004–2023).</p>
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<p>Illustration of spatiotemporal variation in average wind speed and direction calculated at (50 m) during autumn (2004–2023).</p>
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<p>Illustration of spatiotemporal variation in average wind speed and direction calculated at (50 m) during spring (2004–2023).</p>
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<p>Illustration of spatiotemporal variation in average wind speed and direction calculated at (50 m) during spring (2004–2023).</p>
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<p>Illustration of spatiotemporal variation in average wind speed and direction calculated at (50 m) during winter (2004–2023).</p>
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<p>(<b>a</b>): Original wind time−series data. (<b>b</b>) Wind data after taking transformation. (<b>c</b>) One−step−ahead forecast comparison from ARIMA models based on RMSE criteria. The red line indicates the forecasted values from the best-selected model. (<b>d</b>) Expected forecasted wind speed from the ARIMA model. (<b>e</b>) One−step-ahead forecast comparison from SARIMA models based on RMSE criteria. The red line indicates the forecasted values from the best-selected model (<b>f</b>) Expected forecasted wind speed from the SARIMA models.</p>
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27 pages, 2655 KiB  
Article
Mathematical Model for Assessing New, Non-Fossil Fuel Technological Products (Li-Ion Batteries and Electric Vehicle)
by Igor E. Anufriev, Bulat Khusainov, Andrea Tick, Tessaleno Devezas, Askar Sarygulov and Sholpan Kaimoldina
Mathematics 2025, 13(1), 143; https://doi.org/10.3390/math13010143 - 2 Jan 2025
Viewed by 587
Abstract
Since private cars and vans accounted for more than 25% of global oil consumption and about 10% of energy-related CO2 emissions in 2022, increasing the share of electric vehicle (EV) ownership is considered an important solution for reducing CO2 emissions. At [...] Read more.
Since private cars and vans accounted for more than 25% of global oil consumption and about 10% of energy-related CO2 emissions in 2022, increasing the share of electric vehicle (EV) ownership is considered an important solution for reducing CO2 emissions. At the same time, reducing emissions entails certain economic losses for those countries whose exports are largely covered by the oil trade. The explosive growth of the EV segment over the past 15 years has given rise to overly optimistic forecasts for global EV penetration by 2050. One of the major obstacles to such a development scenario is the limited availability of resources, especially critical materials. This paper proposes a mathematical model to predict the global EV fleet based on the limited availability of critical materials such as lithium, one of the key elements for battery production. The proposed model has three distinctive features. First, it shows that the classical logistic function, due to the specificity of its structure, cannot correctly describe market saturation in the case of using resources with limited serves. Second, even the use of a special multiplier that describes the market saturation process taking into account the depletion (finiteness) of the used resource does not obtain satisfactory economic results because of the “high speed” depletion of this resource. Third, the analytical solution of the final model indicates the point in time at which changes in saturation rate occur. The latter situation allows us to determine the tracking of market saturation, which is more similar to the process that is actually occurring. We believe that this model can also be validated to estimate the production of wind turbines that use rare earth elements such as neodymium and dysprosium (for the production of powerful and permanent magnets for wind turbines). These results also suggest the need for oil-exporting countries to technologically diversify their economies to minimize losses in the transition to a low-carbon economy. Full article
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<p>Y/Y growth rate of electric car stock (BEV + PHEV) globally (black line) and in selected countries (red line), based on [<a href="#B13-mathematics-13-00143" class="html-bibr">13</a>,<a href="#B45-mathematics-13-00143" class="html-bibr">45</a>,<a href="#B46-mathematics-13-00143" class="html-bibr">46</a>].</p>
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<p>Global lithium production from 1985 onwards. Source: [<a href="#B50-mathematics-13-00143" class="html-bibr">50</a>,<a href="#B51-mathematics-13-00143" class="html-bibr">51</a>].</p>
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<p>Recent annual average price behavior of lithium between 2010 and 2023. Source: [<a href="#B50-mathematics-13-00143" class="html-bibr">50</a>,<a href="#B51-mathematics-13-00143" class="html-bibr">51</a>].</p>
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<p>Two practically identical approximations of the data of the logistic type (1) where <span class="html-italic">T</span><sub>0</sub> = 2031 (5) and <span class="html-italic">T</span><sub>0</sub> = 2035 (6) (developed by authors).</p>
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<p>Behavior of two logistic functions up to 2060 (see also <a href="#mathematics-13-00143-f004" class="html-fig">Figure 4</a>).</p>
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<p>Evaluation of the approximation quality: SSE criteria (<b>top</b>), R2 (<b>center</b>) and constraint error (<b>bottom</b>).</p>
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<p>Forecast examples for (<b>a</b>) <math display="inline"><semantics> <mrow> <msub> <mi>t</mi> <mi>M</mi> </msub> <mo>=</mo> <mn>2035</mn> </mrow> </semantics></math> and (<b>b</b>) <math display="inline"><semantics> <mrow> <msub> <mi>t</mi> <mi>M</mi> </msub> <mo>=</mo> <mn>2041</mn> </mrow> </semantics></math>.</p>
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<p>Forecast corresponding to the best approximation according to the SSE criterion.</p>
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<p>Predicting EV penetration using the integro-differential Equation (8) (developed by authors).</p>
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<p>Comparison of analytical and numerical solutions of Equation (13) for one model example.</p>
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<p>Results of forecasting the number of EVs using the solution of Equation (13).</p>
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26 pages, 8196 KiB  
Article
Control Strategy for DC Micro-Grids in Heat Pump Applications with Renewable Integration
by Claude Bertin Nzoundja Fapi, Mohamed Lamine Touré, Mamadou-Baïlo Camara and Brayima Dakyo
Electronics 2025, 14(1), 150; https://doi.org/10.3390/electronics14010150 - 2 Jan 2025
Viewed by 487
Abstract
DC micro-grids are emerging as a promising solution for efficiently integrating renewable energy into power systems. These systems offer increased flexibility and enhanced energy management, making them ideal for applications such as heat pump (HP) systems. However, the integration of intermittent renewable energy [...] Read more.
DC micro-grids are emerging as a promising solution for efficiently integrating renewable energy into power systems. These systems offer increased flexibility and enhanced energy management, making them ideal for applications such as heat pump (HP) systems. However, the integration of intermittent renewable energy sources with optimal energy management in these micro-grids poses significant challenges. This paper proposes a novel control strategy designed specifically to improve the performance of DC micro-grids. The strategy enhances energy management by leveraging an environmental mission profile that includes real-time measurements for energy generation and heat pump performance evaluation. This micro-grid application for heat pumps integrates photovoltaic (PV) systems, wind generators (WGs), DC-DC converters, and battery energy storage (BS) systems. The proposed control strategy employs an intelligent maximum power point tracking (MPPT) approach that uses optimization algorithms to finely adjust interactions among the subsystems, including renewable energy sources, storage batteries, and the load (heat pump). The main objective of this strategy is to maximize energy production, improve system stability, and reduce operating costs. To achieve this, it considers factors such as heating and cooling demand, power fluctuations from renewable sources, and the MPPT requirements of the PV system. Simulations over one year, based on real meteorological data (average irradiance of 500 W/m2, average annual wind speed of 5 m/s, temperatures between 2 and 27 °C), and carried out with Matlab/Simulink R2022a, have shown that the proposed model predictive control (MPC) strategy significantly improves the performance of DC micro-grids, particularly for heat pump applications. This strategy ensures a stable DC bus voltage (±1% around 500 V) and maintains the state of charge (SoC) of batteries between 40% and 78%, extending their service life by 20%. Compared with conventional methods, it improves energy efficiency by 15%, reduces operating costs by 30%, and cuts CO2; emissions by 25%. By incorporating this control strategy, DC micro-grids offer a sustainable and reliable solution for heat pump applications, contributing to the transition towards a cleaner and more resilient energy system. This approach also opens new possibilities for renewable energy integration into power grids, providing intelligent and efficient energy management at the local level. Full article
(This article belongs to the Special Issue Innovative Technologies in Power Converters, 2nd Edition)
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<p>Configuration of the proposed micro-grid.</p>
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<p>Electrical architecture of PV system.</p>
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<p>Electrical design of a single diode PV cell.</p>
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<p>The P-V curves showing MPP: (<b>a</b>) fixed temperature and variable irradiance, (<b>b</b>) variable temperature and constant irradiance.</p>
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<p>Basic electrical diagram of the DC-DC boost converter.</p>
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<p>Equivalent electrical design of a single diode PV cell: (<b>a</b>) ON state of the switch, (<b>b</b>) OFF state of the switch.</p>
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<p>Flowchart of the FSCC approach.</p>
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<p>Improved FSCC-MPC algorithm.</p>
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<p>Schematic diagram of wind generator system.</p>
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<p>Schematic diagram of battery energy storage system.</p>
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<p>Wiring diagram for bidirectional DC-DC converter.</p>
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<p>Schematic diagram of the heat pump system.</p>
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<p>Control strategy of the micro-grid-based HP system.</p>
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<p>MPC block diagram of the micro-grid-based HP system.</p>
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<p>Proposed control strategy of the micro-grid-based HP system.</p>
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<p>Measured profiles during the year: (<b>a</b>) solar irradiance, (<b>b</b>) ambient temperature, (<b>c</b>) wind speed.</p>
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<p>Measured profiles over the year: (<b>a</b>) water temperature, (<b>b</b>) heat pump temperature.</p>
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<p>Simulation result of MPC performance: (<b>a</b>) DC bus voltage, (<b>b</b>) battery <span class="html-italic">SoC</span>.</p>
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<p>The different power waveforms: (<b>a</b>) power of PV, (<b>b</b>) power of wind, (<b>c</b>) power of battery, (<b>d</b>) power of heat pump.</p>
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<p>The different power waveforms: (<b>a</b>) over the year, (<b>b</b>) zooming 1, (<b>c</b>) zooming 2.</p>
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